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首页> 外文期刊>Journal of Archaeological Science >Joint geophysical measurements to investigate the Rossano of Vaglio archaeological site (Basilicata Region, Southern Italy)
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Joint geophysical measurements to investigate the Rossano of Vaglio archaeological site (Basilicata Region, Southern Italy)

机译：联合地球物理测量，以调查瓦格里奥考古遗址（意大利南部巴斯利卡塔地区）的罗萨诺

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摘要

A high resolution geophysical survey was carried out in the archaeological site of Rossano di Vaglio (Basilicata Region, Southern Italy), where an important ancient sanctuary is located. It was built during the IV century B.C. and devoted to the goddess Mephitis. The sanctuary rises in an area affected by a multiple and retrogressive rototraslational landslide, historically and presently subject to reactivation. The main objective of this work was the identification of buried structures of archaeological interest in an area designated by the Archaeological Superintendence of the Basilicata Region. The study was performed by means of the use of high resolution geophysical surveys. In particular, we made use of the joint application of three highly sensitive and non-invasive geophysical techniques, namely the Geoelectrical, the Magnetic and the Ground Probing Radar (GPR) methodologies. In such a way, we obtained two important results: first, we provided the archaeologists with information about the limits of the areas to be excavated; second, we could verify in real time the reliability of the geophysical results. The experimental results showed four main magnetic anomalies in the area of study, in agreement with the GPR results obtained for the same target. Finally, a partial excavation test of the investigated area revealed a buried building structure, located in correspondence of an anomaly identified by means of the geophysical prospecting.
机译：在Rossano di Vaglio（意大利南部巴斯利卡塔地区）的考古遗址上进行了高分辨率的地球物理调查，该遗址位于重要的古代保护区。它建于公元前四世纪并致力于女神性肾炎。避难所在受多重和渐进式旋转横断面滑坡影响的区域中兴起，历史上和现在都需要重新活化。这项工作的主要目的是在巴斯利卡塔地区考古监督所指定的地区确定考古感兴趣的埋藏结构。该研究是通过使用高分辨率地球物理调查进行的。特别是，我们利用了三种高度敏感的非侵入性地球物理技术的联合应用，即地电，磁和地面探测雷达（GPR）方法。通过这种方式，我们获得了两个重要结果：首先，我们为考古人员提供了有关待发掘区域范围的信息;其次，我们可以实时验证地球物理结果的可靠性。实验结果表明，该研究领域出现了四个主要的磁异常，与针对同一目标获得的GPR结果一致。最后，对被调查区域的局部挖掘测试揭示了一个埋藏的建筑结构，该结构与通过地球物理勘探确定的异常对应。

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